然后是在1963年，在板块构造理论发展的早期。
Then in 1963, in the early days of the development of the theory of plate tectonics.
威尔逊对这些数据的分析现在是板块构造学的核心部分。
Wilson's analysis of these data is now a central part of plate tectonics.
魏格纳的概念与后来被广泛接受的板块构造理论之间有相当大的重叠。
There is a considerable overlap between Wegener's concepts and the later widely embraced plate tectonics theory.
因此，近年来，一些地质学家会利用板块构造理论来进行他们所谓的地质预测。
So, in recent years, some geologists have used plate tectonic theory to make what they call geopredictions.
然而，板块构造不能完全解释某些巨大的地表特征，例如非洲南部的“superswell”，即一个直径超过1000英里、高度接近1英里的巨大高原。
However, plate tectonics cannot fully explain certain massive surface features, such as the "superswell" of southern Africa, a vast plateau over 1,000 miles across and nearly a mile high.
这板块构造学说的理论讲些什么？
板块构造理论是古板块分区的基础。
The theory of plate tectonics is the division of palaeo-plates.
如今板块构造几乎被普遍接受。
阐明了地幔柱构造与板块构造的关系。
The relation between mantle plume and plate motion is summarized.
板块构造体系说明洋壳俯冲极性从南向北。
The plate tectonic regime suggests the subduction sense from south to north.
预测岛屿未来的变化同时需要考虑板块构造。
Forecast islands future changes at the same time need to consider plate tectonics.
这样在海洋表面的碳酸盐的沉积物通过板块构造返回地球中。
This makes carbonate sediments on the floor of the ocean that are subducted back into the Earth though plate tectonics.
以后的研究经过了地槽理论阶段和板块构造理论阶段。
The research work consequently experienced geosyncline theory period and plate tectonics theory period.
在板块构造不同演化阶段，形成的矿床组合也各不相同；
During the different evolutionary phase of the plate tectonition, there were different deposit associations.
科学家建立了一个能解释大多数地震发生的理论，叫做板块构造。
Scientists have developed a theory, called plate tectonics, that explains why most earthquakes occur.
大陆地壳长时期内未受到板块构造的或造山活动的很多影响的稳定区。
A stable area of continental crust that has not undergone much plate tectonic or orogenic activity for a long period.
板块构造图片美术馆。一条粘鱼类游近管蠕虫在中大西洋山脊在大西洋。
Photo Gallery: Plate Tectonics an eelpout fish swims near tube worms at the Mid-Atlantic Ridge in the Atlantic Ocean.
青藏高原大地构造研究实践表明，青藏高原是板块构造登陆的研究基地。
The study of tectonics on the Qinghai-Tibetan Plateau indicates that the Qinghai-Tibetan Plateau is the ideal research base of the plate-tectonic theory landing on the continent.
板块构造学主要在于探索岩石田块体的运动，属于动力大地构造学范畴。
Plate tectonics explores primarily the motion of lithospheric blocks and belongs to the category of dynamic geotectonics.
科学家发现，板块构造不仅能够解释大陆的漂移，而且能够解释地震的成因。
Scientists realized that plate tectonics might explain not only the drifting apart of continents but also the cause of earthquakes.
使用新算法，科学家们能够模拟全球地幔流动以及它是如何显明板块构造和断层移动的。
With the new algorithms, the scientists were able tosimulate global mantle flow and how it manifests as plate tectonics and themotion of individual faults.
分析造山带中盆地系的板块构造时，需要将靠近作用与分离作用仔细区分开来。
Plate tectonic analysis of basin systems interspersed in orogenic belts requires that the effects of approximation be carefully distinguished from those of separation.
这一构造-岩浆作用暗示着松嫩地块北缘在新元古代板块构造体制就开始运行。
The tectonic magmatism suggests that the plate tectonics had operated in the north margin of Songnen Massif in the Neoproterozoic.
大洋岩石圈与大陆岩石圈之间的多岛弧盆系构造域是板块构造登陆的入门向导。
The rudimental guide of the plate-tectonic theory landing on continent is the archipelagic arc-basin system between the oceanic lithosphere and continental lithosphere.
地球最大的优点在于板块构造，这些构造能够平衡大气层中二氧化碳的数量，使地球保持温暖。
Earth's biggest advantage comes from having plate tectonics that stabilize the amount of carbon dioxide in the atmosphere that keeps Earth warm.
它被分为四个主要的部分：板块构造学，地震，全球定位系统和起作用的空间技术。
It is divided into four major sections: Plate Tectonics, Earthquakes, GPS, and Space Technology at Work.
分析了全球密度异常与板块构造的关系，探讨了全球密度异常分布对板块运动的作用。
The relation between global density anomalies and plate tectonics is discussed. And the action of density anomalies to plate moving is analyzed also.
根据研究人员的该项预测，板块构造的净效应，将使得瓦胡岛在150万年内继续增长。
According to the forecast of the researchers, the net effect of plate tectonics, makes Oahu continue to grow in 150 million years.
板块构造学的工作就是要揭示那快照的线索，了解它的舞步，确定舞蹈者曾去过和将要去哪里。
The job of plate tectonics is to unravel the clues in that snapshot to learn the dance steps to determine where the dancers have been and where they are going.
板块构造学的工作就是要揭示那快照的线索，了解它的舞步，确定舞蹈者曾去过和将要去哪里。
The job of plate tectonics is to unravel the clues in that snapshot to learn the dance steps to determine where the dancers have been and where they are going.
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